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Identifier: rendiconti52111912acca (find matches)
Title: Rendiconti
Year: 1892 (1890s)
Authors: Accademia nazionale dei Lincei. Classe di scienze fisiche, matematiche e naturali
Subjects: Science
Publisher: Roma
Contributing Library: Smithsonian Institution Libraries
Digitizing Sponsor: Biodiversity Heritage Library

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miscugli fra il 32 e lll°/o di Cu2S. Lattacco è stato fatto conpotassa caustica diluita; il metasolfoantimonito è il costituente chiaro. Chimica-fisica. — Ricerche sui seleniti asimmetrici. Sui pro-dotti di addizione della piperidina cogli acidi selenioso e solfo-roso. Nota II di L. Marino e A. Toninelli, presentata dal SocioR. Nasini. Chimica-fisica — Solubilità allo stato solido tra solfati ecarbonati ad alta temperatura. Nota di Mario Amadori, pre-sentata dal Socio G-. Ci amici an. Chimica. — Analisi termiche di miscele binarie di cloruri dielementi monovalenti. Nota IV di C. Sandonnini e G. Scarpa,presentata dal Socio G. Ciamician. Chimica agricola. — Azione del fosfato monocalcico nellaconservazione dei foraggi verdi. Nota di G. Sani, presentatadal Socio G. Kòrner. Le Note precedenti saranno pubblicate nel prossimo fascicolo. (y) Proceed. Kon. Acad. v. Wet. Amsterdam (1911) 510. RENDICONTI DELLA R. ACCADEMIA DEI LINCEI (CI. d. se. fis. ecc.) Voi. XXI, 1° seni. 1912.
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Cu2S 32.10 /„ X70 Cn2S 16.66 o/o — 803 — Petrografia. — Sulla natura delle masse pirosseniche in rela-zione con i giacimenti ferriferi di Rio e Capo Calamita. Nota deldott. Alessandro Martelli, presentata dal Socio Carlo De Stefani. I rnetasilicati che nella parte orientale dellElba si trovano in connes-sione con i giacimenti ferriferi, presentandosi come formazioni di contattofra le masse del minerale coltivato e le rocce sedimentarie, presso la Torredi Rio e a Capo Calamita mostrano con maggiore evidenza che altrove laloro sostituzione al calcare. Compresi in ragguardevoli masse di pirossenotìbroso-raggiato con epidoto, ilvaite e raro granato, si hanno infatti nume-rosi banchi di calcari risparmiati dalle azioni metamorfiche da cui dettisilicati sono evidentemente derivati, mantenendo la disposizione stratigraficadei calcari circostanti e degli stessi strati che rappresentano chiaramente iresidui della formazione calcarea che i silicati hanno sostituita in seguito a

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1912
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30 July 2014

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